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Geochronology of the Dovyren intrusive complex, northwestern Baikal area, Russia, in the Neoproterozoic


Ariskin, AA and Kostitsyn, YA and Konnikov, EG and Danyushevsky, LV and Meffre, SJM and Nikolaev, GS and McNeill, A and Kislov, EV and Orsoev, DA, Geochronology of the Dovyren intrusive complex, northwestern Baikal area, Russia, in the Neoproterozoic, Geochemistry International, 51, (11) pp. 859-875. ISSN 0016-7029 (2013) [Refereed Article]

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Copyright 2013 Pleiades Publishing

DOI: doi:10.1134/S0016702913110025


The paper reports newly obtained data on the geochronology of the Dovyren intrusive complex and associated metarhyolites of the Inyaptuk Formation in the Synnyr Range. The data were obtained by local LA-ICPMS analysis of zircons in samples. The U-Pb age of olivine-free gabbronorite from near the roof of the Yoko-Dovyren Massif is 730 6 Ma (MSWD = 1.7, n = 33, three samples) is close to the estimated age of 731 4 Ma (MSWD = 1.3, n = 56, five samples) of a 200-m-thick sill beneath the pluton. These data overlap the age of recrystallized hornfels found within the massif ("charnockitoid", 723 7 Ma, MSWD = 0.12, n = 10) and a dike of sulfidated gabbronorite below the bottom of the massif (725 8 Ma, MSWD = 2.0, n = 15). The estimates are also consistent with the age of albite hornfels (721 6 Ma, MSWD = 0.78, n = 12), which was produced in a low-temperature contact metamorphic facies of the host rocks. The average age of the Dovyren Complex is 728.4 3.4 Ma (MSWD = 1.8, n = 99) based on data on the sill, near-roof gabbronorite, and "charnockitoid") and is roughly 55 Ma older than the estimate of 673 22 Ma (Sm-Nd; [13]). The U-Pb system of zircon in two quartz metaporphyre samples from the bottom portion of the Inyaptuk volcanic formation in the northeastern part of the Yoko-Dovyren Massif turns out to be disturbed. The scatter of the data points can be explained by the effect of two discrete events. The age of the first zircon population is then 729 14 Ma (MSWD = 0.74, n = 8), and that of the second population is 667 14 Ma (MSWD = 1.9, n = 13). The older value pertains to intrusive rocks of Dovyren, and the age of the "rejuvenated" zircon grains corresponds to the hydrothermal-metasomatic processes, which affected the whole volcano-plutonic sequence and involved the serpentinization of the hyperbasites. This is validated by the results of Rb-Sr isotopic studies with the partial acid leaching of two serpentinized peridotite samples from the Verblyud Sill. These studies date the overprinted processes at 659 5 Ma (MSWD = 1.3, n = 3).

Item Details

Item Type:Refereed Article
Keywords:layered massif, intrusive complex, geochronology, zircon, laser ablation, LA
Research Division:Earth Sciences
Research Group:Geology
Research Field:Geochronology
Objective Division:Expanding Knowledge
Objective Group:Expanding knowledge
Objective Field:Expanding knowledge in the earth sciences
UTAS Author:Danyushevsky, LV (Professor Leonid Danyushevsky)
UTAS Author:Meffre, SJM (Professor Sebastien Meffre)
UTAS Author:McNeill, A (Dr Andrew McNeill)
ID Code:89101
Year Published:2013
Web of Science® Times Cited:47
Deposited By:Centre for Ore Deposit Research - CODES CoE
Deposited On:2014-02-25
Last Modified:2014-05-27
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